Deglacial to Holocene environmental changes in the northern Ligurian Sea: The dual influence of regional climate variability and large-scale intermediate Mediterranean circulation
|Author(s)||Le Houedec Sandrine1, Mojtahid Meryem1, Ciobanu Maria Cristina2, Jorry Stephan2, Bouhdayad Fatima Zohra3, Guyonneau Emma1, Sourice Stéphane1, Toucanne Samuel2|
|Affiliation(s)||1 : LPG-BIAF UMR-CNRS 6112, UNIV Angers, CNRS, 2 bd Lavoisier, 49045 Angers Cedex 01, France
2 : IFREMER, Unité de Recherche Géosciences Marines, Laboratoire Géodynamique et enregistrement Sédimentaire, CS10070, F-29280 Plouzané, France
3 : Institute of Geology and Mineralogy, Faculty of Mathematics and Natural Sciences, University of Cologne, Otto-Fischer-Straße 14, 50674 Cologne, Germany
|Source||Palaeogeography Palaeoclimatology Palaeoecology (0031-0182) (Elsevier BV), 2021-08 , Vol. 576 , P. 110500 (21p.)|
|Keyword(s)||Foraminifera, Paleoclimatology, Western Mediterranea, Holocene|
The sedimentary archives of the Mediterranean Sea record periodic deposits of organic-rich deposits, called sapropels in the eastern basin and organic-rich layers (ORL) in the western basin. Changes in both the Mediterranean circulation and inputs of fresh water through borderlands rivers under more humid climate, are important mechanisms to explain those events. The last ORL and sapropel S1 have different timing, respectively from ~14.5 to 9 Ka and from ~10 to 6 Ka, presumably due to different forcing factors in the western basin (i.e., melting of Alps ices). Here we present a high-resolution study of a marine sediment core located off the mouth of the Var River, one of the most dynamic river system of the northern borderland of the western Mediterranean Sea. We applied a multi-proxy approach based on benthic foraminiferal assemblages, foraminiferal δ18O and δ13C, grain size analyses, organic carbon content and XRF elemental data to decipher the regional climate signals from the basin-scale intermediate circulation signature. Our results do not show large river inputs at the timing of the last ORL deposit. On the opposite, foraminiferal and geochemical evidence indicate that the 11–6 kyr period, concomitant to Sapropel S1 event in the Eastern Mediterranean, was characterised by high river activity and low ventilated bottom waters at the studied location. Additionally, our results characterized the last 6 ka with large scale episodes of more active bottom water ventilation due perhaps to enhanced wind activity under an overall cooler climate.
Time series analyses were computed from stable isotopes, Ca/Ti XRF ratio and foraminifera abundances. They show common frequencies peaks (2.2–3, 1.1–1.2, 0.9–1.0, and 0.4–0.5 kyr) most likely related to the solar activity. Also, a specific frequency band (1.5–1.6 kyr) was only recorded in benthic foraminiferal abundance and stable isotopic records. This was preferentially attributed to an oceanic-driven internal forcing.